Permian of China
The interval definitions in this timescale are derived from the following sources:
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- J. I. Raine, A. G. Beu, A. F. Boyes, H. J. Campbell, R. A. Cooper, J. S. Crampton, M. P. Crundwell, C. J. Hollis, and H. E. G. Morgans. 2015. Revised Calibration of the New Zealand Geological Timescale: NZGT2015/1. GNS Science Report 2012(39) view
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- A. G. Sennikov and V. K. Golubev. 2006. Vyazniki Biotic Assemblage of the Terminal Permian. Paleontological Journal 40(suppl. 4):S475-S481 view
There are 16 timescales which overlap this one. show
Interval boundaries marked with * have been interpolated based on the differences between the ages for international timescale boundaries quoted in the source and the currently accepted ages for those boundaries.
Interval names marked with † are no longer in current use.
This timescale is used in the definition of 42 collections
| International Chronostratigraphic Timescale | Permian of China | Permian-Jurassic of New Zealand | Carboniferous of North America | Permian of the Salt Range | Obsolete Carboniferous Ages of China | Permo-Triassic Subages of Eastern Europe | ||||
|---|---|---|---|---|---|---|---|---|---|---|
| Jurassic | Late Jurassic | Tithonian | Oteke | Puaroan | 145 | |||||
| Kimmeridgian | 149.2 | |||||||||
| Kawhia | Ohauan | 150 | ||||||||
| Heterian | 154.5 | |||||||||
| Oxfordian | 154.8 | |||||||||
| Middle Jurassic | Callovian | 161.5 | ||||||||
| Temaikan | 164.3 | |||||||||
| Bathonian | 165.3 | |||||||||
| Bajocian | 168.2 | |||||||||
| Aalenian | 170.9 | |||||||||
| Early Jurassic | Toarcian | 174.7 | ||||||||
| Herangi | Ururoan | 176 | ||||||||
| Pliensbachian | 184.2 | |||||||||
| Aratauran | 188.9 | |||||||||
| Sinemurian | 192.9 | |||||||||
| Hettangian | 199.5 | |||||||||
| Triassic | Late Triassic | Rhaetian | Balfour | Otapirian | 201.4 | |||||
| Norian | Warepan | 208.5 | ||||||||
| Otamitan | 217 | |||||||||
| Oretian | 221 | |||||||||
| Carnian | 227 | |||||||||
| Gore | Kaihikuan | 227.5 | ||||||||
| Middle Triassic | Ladinian | 237 | ||||||||
| Etalian | 238 | |||||||||
| Anisian | 242 | |||||||||
| Malakovian | 246 | |||||||||
| Early Triassic | Olenekian | Vokhmian | 247.2 | |||||||
| Nelsonian | 249 | |||||||||
| Induan | 251.2 | |||||||||
| DUrville | Makarewan | Kathwai | 251.5 * | |||||||
| Permian | Lopingian | Changhsingian | Meishanian | 251.902 | ||||||
| 252.4 * | ||||||||||
| Chhidru | 252.9 * | |||||||||
| Waiitian | 253.2 | |||||||||
| Baoqingian | 253.4 * | |||||||||
| Wuchiapingian | Laoshanian | Late Vyatkian/Early Vyatkian | 254.14 | |||||||
| Puruhauan | 254.2 | |||||||||
| Kalabagh | 255 * | |||||||||
| Wargal | 256 * | |||||||||
| Laibinian | 257.7 * | |||||||||
| Guadalupian | Capitanian | Lengwuan | Aparima | Flettian | Late Severodvinian/Early Severodvinian | 259.51 | ||||
| Wordian | Kuhfengian | Late Urzhumian/Early Urzhumian | 264.28 | |||||||
| 265.3 * | ||||||||||
| Barettian | 266 | |||||||||
| Amb | 266.1 * | |||||||||
| Roadian | Late Kazanian/Early Kazanian | 266.9 | ||||||||
| 270.7 * | ||||||||||
| Cisuralian | Kungurian | Luodianian | 273.01 | |||||||
| Mangapirian | 276 | |||||||||
| Artinskian | 283.5 | |||||||||
| Telfordian | 285 | |||||||||
| Longlinian | 285.4 * | |||||||||
| 288.5 | ||||||||||
| Sakmarian | 290.1 | |||||||||
| Asselian | Zisongian | Bursumian † | 293.52 | |||||||
| Carboniferous | Pennsylvanian | Gzhelian | Virgilian | Mapingian † | 298.9 | |||||
| 300.1 | ||||||||||
| Kasimovian | Missourian | 303.7 | ||||||||
| Desmoinesian | 305.9 * | |||||||||
| Moscovian | 307 | |||||||||
| Atokan | 312.7 * | |||||||||
| Bashkirian | 315.2 | |||||||||
| Morrowan | 318.4 * | |||||||||
| Mississippian | Serpukhovian | Chesterian | 323.2 | |||||||
| Visean | 330.9 | |||||||||
| Meramecian | 335.8 * | |||||||||
| Osagean | 343.1 * | |||||||||
| Tournaisian | 346.7 | |||||||||
| Kinderhookian | 351.9 * | |||||||||
| 358.9 | ||||||||||